G
Gregory C. Beroza
Researcher at Stanford University
Publications - 231
Citations - 17782
Gregory C. Beroza is an academic researcher from Stanford University. The author has contributed to research in topics: Aftershock & Slip (materials science). The author has an hindex of 63, co-authored 204 publications receiving 14101 citations. Previous affiliations of Gregory C. Beroza include Massachusetts Institute of Technology.
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Journal ArticleDOI
Non-volcanic tremor and low-frequency earthquake swarms
TL;DR: It is demonstrated that tremor beneath Shikoku, Japan, can be explained as a swarm of small, low-frequency earthquakes, each of which occurs as shear faulting on the subduction-zone plate interface.
Journal ArticleDOI
Seismicity Remotely Triggered by the Magnitude 7.3 Landers, California, Earthquake
David P. Hill,Paul A. Reasenberg,Andrew J. Michael,W.J. Arabaz,Gregory C. Beroza,D. Brumbaugh,James N. Brune,Raúl R. Castro,S. Davis,Diane dePolo,William L. Ellsworth,Joan Gomberg,Stephen C. Harmsen,L. House,S.M. Jackson,M. J. S. Johnston,Lucile M. Jones,Rebecca Hylton Keller,Steve Malone,Luis Munguía,S. Nava,James C. Pechmann,A. Sanford,Robert W. Simpson,Robert B. Smith,M. Stark,Michael C. Stickney,Antonio Vidal,S. Walter,Victor Wong,J. Zollweg +30 more
TL;DR: The most promising explanations involve nonlinear interactions between large dynamic strains accompanying seismic waves from the mainshock and crustal fluids (perhaps including crustal magma).
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Low-frequency earthquakes in Shikoku, Japan, and their relationship to episodic tremor and slip
TL;DR: Strong evidence is provided that these earthquakes occur on the plate interface, coincident with the inferred zone of slow slip, and the locations and characteristics of these events suggest that they are generated by shear slip during otherwise aseismic transients, rather than by fluid flow.
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A scaling law for slow earthquakes
TL;DR: It is shown that these slow events follow a simple, unified scaling relationship that clearly differentiates their behaviour from that of regular earthquakes, and may lead to a better understanding of the plate subduction process and large earthquake generation.
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Shallow Dynamic Overshoot and Energetic Deep Rupture in the 2011 Mw 9.0 Tohoku-Oki Earthquake
TL;DR: Finite-source imaging reveals that the rupture consisted of a small initial phase, deep rupture for up to 40 seconds, extensive shallow rupture at 60 to 70 seconds, and continuing deep rupture lasting more than 100 seconds, which may have enabled large shallow slip near the trench.